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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Journal of solution chemistry 19 (1990), S. 175-185 
    ISSN: 1572-8927
    Keywords: Solubility ; barite ; celestite ; activity coefficient ; equilibrium constants
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Abstract The solubilities of barite [BaSO4(c)] and celestite [SrSO4(c)] in Na2SO4 were studied and found to be significantly lower than the experimental values reported in the literature. Our new solubility data are in excellent agreement with the predictions of ion interaction models, which have previously been parameterized primarily from solubility data obtained in chloride media. Our solubility data were analyzed both in terms of aqueous thermodynamic models that included ion association species and in terms of ion interaction models that did not require the explicit recognition of such species. In the case of SrSO4, although both ion association and ion interaction models can accurately model our solubility data, the ion interaction approach is preferred because it is easier to extend to higher concentrations. In the case of BaSO4, the aqueous ion interactions appear to be stronger than those for SrSO4, and so the explicit recognition of a BaSO4(aq) ion association species is preferred. The logarithms of the thermodynamic solubility products (log K sp ) for celestite and barite were −6.62±0.02 and −10.05±0.05, respectively. When the data were analyzed using models that include ion association species, the logarithms of the thermodynamic equilibrium constants for the SrSO4(aq) and BaSO4(aq) association reactions were 1.86±0.03 and 2.72±0.09, respectively.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1572-8927
    Keywords: Solubility ; equilibrium constants ; activity coefficient ; hydrolysis ; β-Cd(OH)2(c) ; ion-interaction parameters ; cadmium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Abstract The solubility of Cd(OH)2(c) was studied in 0.01M NaClO4 solutions, from both the over- and the undersaturation directions, with OH− ion concentration ranging from 10−6 to 1.0 mol-L−1, and the equilibration period ranging from 2 to 28 days. Equilibrium Cd concentrations were reached in less than 2 days. The Cd(OH)2(c) solubility showed an amphoteric behavior. In the entire range of OH−/H+ investigated, the only dominant aqueous Cd(II) species required to explain the solubility of Cd(OH)2(c) are Cd2+, Cd(OH) 2 0 , and Cd(OH) 4 2− . The logarithms of the thermodynamic equilibrium constants of the Cd(OH)2(c) solubility reactions involving these species, that is, the reactions $$\begin{gathered} {\text{ }}Cd(OH)_2 (c) \rightleftarrows Cd^{2 + } + 20H^ - ,{\text{ }}Cd(OH)_2 (c) \rightleftarrows Cd(OH)_2^0 , \hfill \\ and Cd(OH)_2 (c) + 20H^ - \rightleftarrows Cd(OH)_4^{2 - } \hfill \\ \end{gathered}$$ were found to be −14.14±0.21, −7.04±0.21, and −5.62±0.32, respectively. The ion-interaction parameters reported in the literature, in conjunction with the values for Cd(OH) 2 0 −Na+(−0.20), Cd(OH) 4 2− −Na+ (β0 = 0.41, β1 = 0.7), and Cd(OH) 4 2− −K+ (β0 = 0.44, β1 = 1.44) obtained in this study, show that our low-ionic strength solubility data are also consistent with Cd(OH)2(c) solubility data obtained in solutions as concentrated as 10M in NaOH or KOH and 7M in Na(OH, ClO4).
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Journal of solution chemistry 24 (1995), S. 735-752 
    ISSN: 1572-8927
    Keywords: Solubility ; equilibrium constants ; solubility product ; Fe2(SeO3)3·6H2O(c) ; ferric selenite ; selenite
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Abstract The aqueous solubility of Fe2(SeO3)3·6H2O(c) was studied in deionized water adjusted to a range in pH values from 0.77 to 5.1 and in Na2SeO3 solutions ranging in concentrations from 0.0002 to 0.02 mol-dm−3. The studies were conducted from both the undersaturation and oversaturation directions, with equilibration periods ranging from 7 to 1725 days. Stoichiometric dissolution of the solid was observed in solutions with pH values up to nearly 4. In general, concentrations of both Se and Fe decreased as pH increased from 1 to 4. Analyses of the equilibrated suspensions confirmed the equilibrium solid to be Fe2(SeO3)3·6H2O(c) and the aqueous Se to be selenite. Pitzer's ion-interaction model was used with selected ion pairs to interpret the solubility data. The logarithm of the solubility product of ferric selenite $$Fe_2 (SeO_3 )_3 .6H_2 O(c) \begin{array}{*{20}c} \to \\ \leftarrow \\ \end{array} 2Fe^{3 + } + 3SeO_3^{2 - } + 6H_2 O$$ was found to be −41.58±0.11. This value is less than any reported in the literature for a ferric selenite by more than 10 orders of magnitude. The solubility data and calculations show an extremely strong interaction between aqueous Fe3+ and SeO 3 2− ; interpretation of these data requires the inclusion of FeSeO 3 + i.e. $$Fe^{3 + } + SeO_3^{2 - } \begin{array}{*{20}c} \to \\ \leftarrow \\ \end{array} FeSeO_3^ + , log K = 11.15 \pm 0.11$$
    Type of Medium: Electronic Resource
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